PeterDonis
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mfb said:Deviations from those cycles are slow.
Slower than annual, yes. But there is still plenty of evidence that the key processes involved change significantly on time scales much shorter than 1 kyr. For example, the following papers all describe significant changes in primary CO2 production in the ocean due to biological processes on time scales of a few decades:
http://www.sciencedirect.com/science/article/pii/S0079661115000993
http://onlinelibrary.wiley.com/doi/10.1029/2010GB004026/full
https://www2.cgd.ucar.edu/sites/default/files/asp-colloquium/files/Chavez-Messie-etal-2011.pdf
http://onlinelibrary.wiley.com/doi/10.1029/2010GB004026/full
Also, rates of upwelling are known to vary significantly on decadal timescales (I don't have any links handy at the moment but can find some if desired).